利用时域求解器进行拉普拉斯域无串扰源编码弹性全波形反演

GEOPHYSICS Pub Date : 2024-04-10 DOI:10.1190/geo2023-0351.1
Z. Liu, Jürgen Hoffmann, Etienne Bachmann, Congyue Cui, Frederik J. Simons, J. Tromp
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引用次数: 0

摘要

使用时域求解器的无串扰震源编码弹性全波形反演(FWI)在利用有限的计算资源进行涉及多个震源和接收器的地震反演方面表现出了技术和效率。该程序的常见公式的一个缺点是,通过以每个镜头一个或几个稀疏采样频率的速率随机扫描频域,很难同时纳入时间选择数据窗口,而这是在反演的各个阶段锁定到达或波包所必需的。在这里,我们通过使用数据的拉普拉斯变换来解决这个问题。使用复值频率可以用灵活的衰减率和时间偏移来阻尼记录,从而锁定特定的旅行时间。我们介绍了拉普拉斯域中无串扰源编码 FWI 的理论,制定了其实施细节,并通过与勘探规模场景相关的数值示例说明了该程序。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Laplace-Domain Crosstalk-Free Source-Encoded Elastic Full Waveform Inversion Using Time-Domain Solvers
Crosstalk-free source-encoded elastic Full-Waveform Inversion (FWI) using time-domain solvers has demonstrated skill and efficiency at conducting seismic inversions involving multiple sources and receivers with limited computational resources. A drawback of common formulations of the procedure is that, by sweeping through the frequency domain randomly at a rate of one or a few sparsely sampled frequencies per shot, it is difficult to simultaneously incorporate time-selective data windows, as necessary for the targeting of arrivals or wave packets during the various stages of the inversion. Here, we solve this problem by using the Laplace transform of the data. Using complex-valued frequencies allows for damping the records with flexible decay rates and temporal offsets that target specific traveltimes. We present the theory of crosstalk-free source-encoded FWI in the Laplace domain, develop the details of its implementation, and illustrate the procedure with numerical examples relevant to exploration-scale scenarios.
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